Figure 2: Hydrologic Zones

Total Page:16

File Type:pdf, Size:1020Kb

Figure 2: Hydrologic Zones r Teslin e o r River l in r iv a e az e f v T iv R f i R Tathlina u R k Kusawa B Tazin e Slave in s Trout Lake T l Northwest S a z Lake la Lake Alaska A River v r Lake Buffalo e Rive ffa Beave u lo R R Yukon r r Lake B i Ri v i e ve er v v r e i Territories r e R n d a l r S n Teslin Territory e R r a v t iv l a l i a to e r i F y R t r v Lake C e e Legend c Tagish oa d e L H r P v l a i ia a r R i R d R Lake M R L i iv iv v e e Bistcho e r r r Lake Hydrologic Zone Boundary Atlin ! titot River d r Pe Atlin r e ia Lake iv L L Old MOE Regional BoundarySaskatchewan i R ard T Ri e ver s l i n r Natural ResourceLake Regions: e F Ne R v ort lson R Claire iv i iv e R er Kotcho r ease D Lake 2 Fort ay River er Nelson H h Riv ! Birc Cree r e Clea v rw i i Lake nR ver r Riv a R e i r t a e e v t g i r Cree a R e n h r a Lake w p u k o r r T s ive P R 3K u s e Fonta M 4 c h Hydrologic Zones ik ik a M kw a v R Ri er iv e Zone Number Name R r e iv Stikin e Skeena r Northeast Figure 2: Hydrologic Zonesr e Riv Turnor NORTHERN COAST MOUNTAINS er Fort Cle arw at Lake 1 Region in F lay Region Frobisher R i er McMurray! v r e iv Lake nchaga R e Waba r hi v s r C i ca R e ive STIKINE PLATEAU iv Bea R r R tto ni Chi ef n n 2 Sikan R e o Churchill k o iv No ti w 1 in L e r River Peter Lake iv NORTHERN ROCKY MOUNTAINS lfway R er Pond Lake Ha 3 5 km Iskut River Lac r 0 100 200 300 e 400 ?le-?-la-Crosse NORTHERN INTERIOR PLAINS iv W R aba ristina É 4 sca Ch 6 River ¯ Fort St. ! 5 NORTHERN CENTRAL UPLANDS John Williston Primrose Lake Lesser Lake SOUTHERN INTERIOR PLAINS Slave Lake O 6 m River r ineca ive e R Pin SOUTHERN ROCKY MOUNTAIN FOOTHILLS 7 7 Grande Prairie Beave r ! r Ri e v e r r v i r e piti Rive NECHAKO PLATEAU iv Takla Omineca R Wa R y s L s a i Lake t 8 a r t N r l u e M S Region m Babine o SOUTHERN HAZELTON MOUNTAINS k Alberta y Smithers! Lake R 9 i v B e r ul k l e 8 r CENTRAL COAST MOUNTAINS Prince y r e r e Stuart v ive iv regor i 10 Rupert a R R cG R ! n Lake M r y ee Rive k Sk mo S Edmonton Masset ! B HAIDA GWAII ! attle River 9 Necha Prince ko Ri 11 Morice Fran?ois ver George ! 12 Lake Lake River od Ootsa e MCGREGOR BASIN L Lake c 12 M Pembina River UPPER FRASER BASIN 13 Eutsuk z ra eau River Lake B NORTHERN COLUMBIA MOUNTAINS 11 13 14 10 Red Deer! FRASER PLATEAU C Quesnel 15 h ilc R otin Lake iver r e Williams v SOUTHERN QUESNEL HIGHLAND i R R !Lake e 16 n Kinbasket d D o e Cariboo s er 14 p Lake R ive m r o NORTHERN THOMPSON PLATEAU h 16 T 17 West Coast 25 Region h ort N Calgary! B UPPER COLUMBIA BASIN Region 18 ow River 18 15 Adams Lake K o o Shuswap te Chilko Revelstoke! n Lake a Medicine UPPER KOOTENAY BASIN Lake y R Hat 19 iv ! e r Upper22 Arrow Lake 27 r CENTRAL KOOTENAY BASIN n R e so iv Thompson / p ! 20 m Kamloops o 26 h T Okanagan Kootenay / O LOWER KOOTENAY BASIN 19 l Lethbridge! d ma 21 n 17 Boundary R Region i ver LOWER COLUMBIA BASIN Campbell South Kelowna 22 ! Region River! Kootenay Okanagan Cranbrook! Lake Lake Coast Nelson OKANAGAN HIGHLAND 23 ! 23 Lower 20 28 Region Harrison Arrow Lake 21 29 Lake 24 24 SOUTHERN THOMPSON PLATEAU Vancouver! Nanaimo! 25 EASTERN SOUTH COAST MOUNTAINS 26 CENTRAL SOUTH COAST MOUNTAINS Victoria ! Montana WESTERN SOUTH COAST MOUNTAINS 27 Washington 28 EASTERN VANCOUVER ISLAND Idaho 29 WESTERN VANCOUVER ISLAND.
Recommended publications
  • Gyrfalcon Falco Rusticolus
    Gyrfalcon Falco rusticolus Rob Florkiewicz surveys, this area was included. Eight eyries are known from this Characteristics and Range The northern-dwelling Gyrfalcon is part of the province; however, while up to 7 of these eyries have the largest falcon in the world. It breeds mostly along the Arctic been deemed occupied in a single year, no more than 3 have been coasts of North America, Europe and Asia (Booms et al. 2008). productive at the same time. Based on these data and other Over its range, its colour varies from white through silver-grey to sightings, the British Columbia Wildlife Branch estimates the almost black; silver-grey is the most common morph in British breeding population in the province to be fewer than 20 pairs Columbia. It nests on cliff ledges at sites that are often used for (Chutter 2008). decades and where considerable amounts of guano can accumulate. Ptarmigan provide the Gyrfalcon's main prey in In British Columbia, the Gyrfalcon nests on cliff ledges on British Columbia and productivity appears dependent on mountains in alpine areas, usually adjacent to rivers or lakes. ptarmigan numbers. Large size and hunting prowess make the Occasionally, it nests on cliffs of river banks and in abandoned Gyrfalcon a popular bird with falconers, who breed and train Golden Eagle nests. them to hunt waterfowl and other game birds. Conservation and Recommendations Whilst the Gyrfalcon is Distribution, Abundance, and Habitat Most Gyrfalcons breed designated as Not at Risk nationally by COSEWIC, it is Blue-listed along the Arctic coast; however, a few breed in the northwest in British Columbia due to its small known breeding population portion of the Northern Boreal Mountains Ecoprovince of British (British Columbia Ministry of Environment 2014).
    [Show full text]
  • Physiography Geology
    BRITISH COLUMBIA DEPARTMENT OF MINES HON. W. K. KIERNAN, Minister P. J. MULCAHY, Deputy Minister NOTES ON PHYSIOGRAPHY AND GEOLOGY OF (Bli BRITISH COLUMBIA b OFFICERS OF THE DEPARTMENT VICTCRIA, B.C. 1961 PHYSIOGRAPHY Physiographic divisions and names are established by the Geographic Board of Canada. Recently H. S. Bostock, of the Geological Survey of Canada, studied the physiography of the northern Cordilleran region; his report and maps are published CI I c Fig. 1. Rglief map of British Columbia. in Memoir 247 of the Geological Survey, Department of Mines and Resources, Ottawa. The divisions shown on the accompanying sketch, Figure 2, and the nomenclature used in the text are those proposed by Bostock. Most of the Province of British Columbia lies within the region of mountains and plateaus, the Cordillera of Western Canada, that forms the western border of the North American Continent. The extreme northeastern comer of the Province, lying east of the Cordillera, is part of the Great Plains region. The Rocky Mountain Area extends along the eastern boundary of the Province for a distance of 400 miles, and continues northwestward for an additional 500 miles entirely within the Province. The high, rugged Rocky Mountains, averaging about 50 miles in width, are flanked on the west by a remarkably long and straight valley, known as the Rocky Mountain Trench, and occupied from south to north by the Kootenay, Columbia, Canoe, Fraser, Parsnip, Finlay, Fox, and Kechika Rivers. Of these, the first four flow into the Pacific Ocean and the second four join the Mackenzie River to flow ultimately into the Arctic Ocean.
    [Show full text]
  • Okanagan Range Ecoregion
    Selecting Plants for Pollinators A Guide for Gardeners, Farmers, and Land Managers In the Okanagan Range Ecoregion Keremeos and Hedley Table of CONTENTS Why Support Pollinators? 4 Getting Started 5 Okanagan range 6 Meet the Pollinators 8 Plant Traits 10 Developing Plantings 12 Farms 13 Public Lands 14 Home Landscapes 15 Plants That Attract Pollinators 16 Habitat hints 20 Habitat and Nesting requirements 21 S.H.A.R.E. 22 Checklist 22 This is one of several guides for different regions of North America. Resources and Feedback 23 We welcome your feedback to assist us in making the future guides useful. Please contact us at [email protected] 2 Selecting Plants for Pollinators Selecting Plants for Pollinators A Guide for Gardeners, Farmers, and Land Managers In the Okanagan Range Ecoregion Keremeos and Hedley A NAPPC and Pollinator Partnership Canada™ Publication Okanagan Range 3 Why support pollinators? IN THEIR 1996 BOOK, THE FORGOTTEN POLLINATORS, Buchmann and Nabhan estimated that animal pollinators are needed for the reproduction “Flowering plants of 90% of fl owering plants and one third of human food crops. Each of us depends on these industrious pollinators in a practical way to provide us with the wide range of foods we eat. In addition, pollinators are part of the across wild, intricate web that supports the biological diversity in natural ecosystems that helps sustain our quality of life. farmed and even Abundant and healthy populations of pollinators can improve fruit set and quality, and increase fruit size. In farming situations this increases production per hectare. In the wild, biodiversity increases and wildlife urban landscapes food sources increase.
    [Show full text]
  • Minfile Nts 082Ese - Grand Forks
    MINFILE NTS 082ESE - GRAND FORKS Original release date: 1997 Researched and compiled by: B.N. Church and L.D. Jones The Grand Forks map area, located in south-central British Columbia, contains 261 documented mineral occurrences, including 108 past producers. The map area includes the historically important Greenwood mining camp, which continues to attract exploration interest and activity. Physiographic domains include the Okanagan Highland over most of the map area, and the Selkirk Mountains to the east of Lower Arrow Lake. The map area lies in the Omineca tectonic belt, which formed in Early to Middle Jurassic time as a result of the accretion of Paleozoic and Mesozoic oceanic and arc rocks of the Slide Mountain and Quesnel terranes. These terranes were delaminated from the oceanic lithosphere and stacked against the continental margin of the North America craton. The resulting calc-alkaline plutonism created a large number of Middle Jurassic intrusions of intermediate composition. These intrude the accreted terranes and the Proterozoic pericratonic Monashee Complex. Overprinting by Cretaceous Laramide and post-Laramide Tertiary transtensional structures has complicated the geology. Paleozoic age, unconformable bedded assemblages include the Knob Hill, Attwood and Anarchist groups. Knob Hill Group is Permo-Carboniferous, and possibly as old as Devonian, and consists of massive and banded MINFILE NTS 082ESE - Grand Forks metacherts and lesser amounts of quartz chlorite schist, amphibolitic schists and gneisses, and limestone bands. The rocks have been affected by deformation and metamorphism causing recrystallization and the development of foliation, quartz sweats parallel to foliation and much deformation of individual beds. The Attwood Group is Permian and consists of black argillite, sharpstone conglomerate, greywacke, limestone lenses and metavolcanic units.
    [Show full text]
  • Wapiti River Water Management Plan Summary
    Wapiti River Water Management Plan Summary Wapiti River Water Management Plan Steering Committee February 2020 Summary The Wapiti River basin lies within the larger Smoky/Wapiti basin of the Peace River watershed. Of all basins in the Peace River watershed, the Wapiti basin has the highest concentration and diversity of human water withdrawals and municipal and industrial wastewater discharges. The Wapiti River Water Management Plan (the Plan) was developed to address concerns about water diversions from the Wapiti River, particularly during winter low-flow periods and the potential negative impacts to the aquatic environment. In response, a steering committee of local stakeholders including municipalities, Sturgeon Lake Cree Nation, industry, agriculture, the Department of Fisheries and Oceans Canada, and the Mighty Peace Watershed Alliance (MPWA), supported by technical experts from Alberta Environment and Parks (AEP), was established. The steering committee initiated the development of a water management plan that includes a Water Conservation Objective (WCO) and management recommendations for the Wapiti River basin from the British Columbia border to its confluence with the Smoky River. A WCO is a limit to the volume of water that can be withdrawn from the Wapiti River, ensuring that water flow remains in the river system to meet ecological objectives. The Plan provides guidance and recommendations on balancing the needs of municipal water supply, industry uses, agriculture and other uses, while maintaining a healthy aquatic ecosystem in the Alberta portion of the Wapiti River basin. Wapiti River Water Management Plan | Summary 2 Purpose and Objectives of the Plan The Plan will be provided as a recommendation to AEP and if adopted, would form policy when making water allocation decisions under the Water Act, and where appropriate, under the Environmental Protection and Enhancement Act by establishing a WCO for the Wapiti River.
    [Show full text]
  • British Columbia Coal Industry Overview 2014
    British Columbia Geological Survey Ministry of Energy and Mines www.em.gov.bc.ca/geology British Columbia Coal Industry Overview 2014 Ministry of Energy and Mines, British Columbia Geological Survey Information Circular 2015-03 British Columbia Coal Industry Overview 2014 Ministry of Energy and Mines British Columbia Geological Survey Information Circular 2015-03 Ministry of Energy and Mines Mines and Mineral Resources Division British Columbia Geological Survey Front Cover: Folded coal seam-bearing strata in the lower part of the Gething Formation, Brule Mine (Walter Energy, Inc) Northeast Region. Hammer lower right for scale. Photo by Paul Jago. Back Cover: Mining coking coal from the Gates Formation at the Perry Creek (Wolverine) operation (Walter Energy, Inc). Photo by Paul Jago. This publication is available, free of charge, from the British Columbia Geological Survey website: www.em.gov.bc.ca/geology Victoria British Columbia Canada January 2015 British Columbia Coal Industry Overview 2014 British Columbia Geological Survey Ministry of Energy and Mines Introduction British Columbia coal industry trends in 2014 In 2014, the number of operating coal mines in the province Global coal prices continued to fall in 2014. Premium hard dropped from nine to six as operations at three mines in the coking coal (HCC) dropped to $121 from $155 in 2013, PCI Peace River Coalfi eld were suspended. However, production coal to $107 from $125, and thermal coal to $82 from $95. at the fi ve coal mines in the southeastern part of the province (All prices are per tonne, in $US, Estimated, West Coast port remained steady, and total coal production dipped only slightly price.) Three metallurgical/PCI coal mines in northeast British from 2013 levels.
    [Show full text]
  • Analysis of the Efficacy of Lidar Data As a Tool for Archaeological Prospection at the Highland Valley Copper Mine
    Analysis of the Efficacy of LiDAR Data as a Tool for Archaeological Prospection at the Highland Valley Copper Mine by Sarah K. Smith B.A., University of British Columbia 2005 Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Arts in the Department of Archaeology Faculty of Environment © Sarah K Smith 2021 SIMON FRASER UNIVERSITY Spring 2021 Copyright in this work rests with the author. Please ensure that any reproduction or re-use is done in accordance with the relevant national copyright legislation. Declaration of Committee Name: Sarah K . Smith Degree: Master of Ar ts Title: Analysis of the Efficacy of LiDAR Data as a Tool for Archaeological Prospection at the Highland Valley Copper Mine Committee: Chair: John Welch Professor , Archaeology David Burley Supervisor Professor, Archaeology Kristin Safi Committee Member Senior Archaeologist Wood Environment & Infrastructure Solutions Travis Freeland Examiner Project Manager Kleanza Consulting Ltd. ii Abstract As heritage resource management and Indigenous heritage stewardship moves into the forefront of project design and operational planning in British Columbia, researchers look for innovative ways to foster impact assessment efficiency without sacrificing quality. In this study I explore methods for employing LiDAR-derived digital elevation models as a tool for archaeological prospection within the Highland Valley Copper Mine. A review of contemporary and formative LiDAR-analysis archaeological prospection research was conducted to identify the most appropriate visualization techniques and data management workflow. Specific methods for the identification of microtopographic relief with the potential to contain archaeological resources were developed. The efficacy of LiDAR-based topographic analysis using manual feature extraction is validated through comparison with georeferenced survey and ground-truthing data provided by my research partners at the Nlaka’pamux Nation Tribal Council.
    [Show full text]
  • Basin Architecture of the North Okanagan Valley Fill, British Columbia
    BASIN ARCHITECTURE OF THE NORTH OKANAGAN VALLEY FILL, BRITISH COLUMBIA sandy Vanderburgh B.Sc., University of Calgary I984 M.Sc., University of Calgary 1987 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in the Department of Geography 0 Sandy Vanderburgh SIMON FRASER UNIVERSITY July 1993 All rights reserved. This work may not be reproduced in whole or in part, by photocopy or other means, without permission of the author. APPROVAL ' Name: Sandy Vanderburgh Degree: Doctor of Philosophy Title of Thesis: Basin Architecture Of The North Okanagan Valley Fill, British Columbia Examining Committee: Chair: Alison M. Gill Associate Professor Dr. M.C. Roberts, Protessor Senior Supervisor Idr. H. Hickin, professor Dr. Dirk Tempelman-Kluit, Director Cordilleran Division, Geological Survey of Canada Dr. R.W. Mathewes, Professor, Department of Biological Sciences Internal Examiner Dr. James A. Hunter, Senior scientist & Program Co-ordinator, Terrain Sciences Division Geological Survey of Canada External Examiner Date Approved: Julv 16. 1993 PARTIAL COPYRIGHT LICENSE 8* I hereby grant to Simon Fraser University the right to lend my thesis, projector extended essay (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further agree that permission for multiple copying of this work for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying or publication of this work for financial gain shall not be allowed without my written permission.
    [Show full text]
  • North Thompson Official Community Plan
    Schedule “A” to Bylaw 2700 North Thompson Official Community Plan Foreword and Acknowledgements The North Thompson Official Community Plan is the outcome of over two years of research, public participation and planning. The Regional District is grateful to all those residents and groups who provided interest, passion, and support from all corners of the Plan area culminating in the Plan development. In particular, we wish to recognize the following people for the exceptional amount of time and energy they dedicated to the planning process. OCP Advisory Committee Director Carol Schaffer, Electoral Area “A” Director Stephen Quinn, Electoral Area “B” Director Bill Kershaw, Electoral Area “O” Tom Eustache – Simpcw First Nation Rick Dee Harley Wright Willow Macdonald (past member) Meetings, Conversations and Information Providers Anna Kay Eldridge – Simpcw First Nation Ashley Dyck – Planning Services Celia Nord – Little Shuswap Indian Band Chris Ortner Dan Winiski Doris Laner – North Thompson Arts Council James Demens and Brandon Gustafsen – Ministry of Transportation and Infrastructure Jenny Green and Clare Audet – Interior Health Authority Kelly Funk – Kelly Funk Photography Laura Ryser – Research Manager, Rural and Small Town Studies Program, UNBC Leanne Nystoruk Mike Scarff, TNRD GIS Services PIBC and the Planners from the local Interior Chapter Sarah Cooke and Mike Cloet – Ministry of Mines, Energy and Petroleum Resources Staff and students at Clearwater and Barriere Secondary Schools Staff from the Agricultural Land Commission Staff
    [Show full text]
  • Late Prehistoric Cultural Horizons on the Canadian Plateau
    LATE PREHISTORIC CULTURAL HORIZONS ON THE CANADIAN PLATEAU Department of Archaeology Thomas H. Richards Simon Fraser University Michael K. Rousseau Publication Number 16 1987 Archaeology Press Simon Fraser University Burnaby, B.C. PUBLICATIONS COMMITTEE Roy L. Carlson (Chairman) Knut R. Fladmark Brian Hayden Philip M. Hobler Jack D. Nance Erie Nelson All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording or any information storage and retrieval system, without permission in writing from the publisher. ISBN 0-86491-077-0 PRINTED IN CANADA The Department of Archaeology publishes papers and monographs which relate to its teaching and research interests. Communications concerning publications should be directed to the Chairman of the Publications Committee. © Copyright 1987 Department of Archaeology Simon Fraser University Late Prehistoric Cultural Horizons on the Canadian Plateau by Thomas H. Richards and Michael K. Rousseau Department of Archaeology Simon Fraser University Publication Number 16 1987 Burnaby, British Columbia We respectfully dedicate this volume to the memory of CHARLES E. BORDEN (1905-1978) the father of British Columbia archaeology. 11 TABLE OF CONTENTS Page Acknowledgements.................................................................................................................................vii List of Figures.....................................................................................................................................iv
    [Show full text]
  • BUILDING the FUTURE NOW
    CONFERENCE September 24 – September 28 Calgary, Alberta, Canada Book of Abstracts BUILDING the FUTURE NOW Abstracts Book Sponsored by http://www.internationalpipelineconference.com IPC is co-owned by ASME and CEPA 12th International Pipeline Conference September 24 – September 28, 2018 Calgary, Alberta, Canada BOOK OF ABSTRACTS Copyright © 2018 by ASME The American Society of Mechanical Engineers Three Park Avenue, New York, NY 10016-5990 2 Copyright © 2018 by ASME - 2 - COPYRIGHT INFORMATION Book of Abstracts from papers accepted for presentation at the 2018 12th International Pipeline Conference (IPC2016) September 24-28, 2018 • Calgary, Alberta, Canada © 2018 ASME All rights reserved ASME shall not be responsible for statements or opinions advanced in papers or discussion at meetings of ASME or its Divisions or Sections, or printed in its publications (Statement from ASME By-Laws, 7.1.3). ASME Presenter Attendance Policy Papers not presented at the conference, by an author of the paper, will not be published in the official archival proceedings. It will also not be published in the ASME Digital Collection and may not be cited as a published paper. As such, the abstracts in this compilation do not represent the final abstracts of the official proceedings. Abstracts are provided courtesy of ASME. The content in this Abstract Book is for personal use only, and cannot be distributed without permission from ASME. Copyright © 2018 by ASME 3 - 3 - Welcome Welcome 2018 IPC CHAIR WELCOME MESSAGE On behalf of the International Pipeline Conference (IPC) Organizing Committee, we are excited to welcome you to IPC 2018 on September 24 – 28 in Calgary, Alberta, Canada.
    [Show full text]
  • Okanagan Ecoregional Assessment  Volume 1  Report
    VOLUME Okanagan 1 Ecoregional Assessment REPORT October 2006 OKANAGAN ECOREGIONAL ASSESSMENT VOLUME 1 REPORT Okanagan Ecoregional Assessment October 2006 Prepared by Nature Conservancy of Canada The Nature Conservancy of Washington and the Washington Department of Fish and Wildlife OKANAGAN ECOREGIONAL ASSESSMENT VOLUME 1 REPORT Okanagan Ecoregional Assessment Volume 1 – Report Citation: Pryce, B., P. Iachetti, G. Wilhere, K. Ciruna, J. Floberg, R. Crawford, R. Dye, M. Fairbarns, S. Farone, S. Ford, M. Goering, M. Heiner, G. Kittel, J. Lewis, D. Nicolson, and N. Warner. 2006. Okanagan Ecoregional Assessment, Volume 1 – Report. Prepared by Nature Conservancy of Canada, The Nature Conservancy of Washington, and the Washington Department of Fish and Wildlife with support from the British Columbia Conservation Data Centre, Washington Department of Natural Resources Natural Heritage Program, and NatureServe. Nature Conservancy of Canada, Victoria, British Columbia. Cover Design: Paul Mazzucca Copyright © 2006 Nature Conservancy of Canada Vancouver, British Columbia Issued by: The Nature Conservancy of Canada Cover Photo Credits: #300 – 1205 Broad Street Methow Valley, Robin Dye; Western screech owl, Victoria, British Columbia, Canada V8W 2A4 A.M. Bezener/One Wild Earth Photography; Great Email: [email protected] basin spadefoot toad, A.M. Bezener/One Wild Earth Photography; Seton Lake, Ian Routley; Canadian Cataloguing in Publication Data: Townsends big-eared bat, Harry van Oort; Mormon metalmark, Orville Dyer; East Chopaka, ISBN 1-897386-00-1 Barbara Pryce; Mountain bluebird, Ian Routley; 1. Biological inventory and assessment – Sockeye salmon, Kristy Ciruna; Badgers, Philippe Okanagan. Verkerk; Lynx, Grant Merrill; Mountain lady’s I. Nature Conservancy of Canada. slipper, George Thornton; Long-billed curlew, Ian II.
    [Show full text]